Land use change Flashcards

1
Q

How have krill responded to warming oceans

A

Moved about 400km further south towards pole. This will affect the animals that feed on them.

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2
Q

Draw the land use transitions graph

A

P.O.P

We are changing the climate by changing the landscape eg urban heat island affect, deforestation increasing albedo etc

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3
Q

Draw how we can trade off growing crops with ecosystem services

A

pop.

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4
Q

Why is the arctic under increasing threat

A

Development, road construction, pipelines etc

For example the road from Inuvik to Tuktoyaktuk in Canada. Build with ice crystal and gravel in winter. Then waiting and in summer it settled then melts. They put loads of insulation in the bottom so warm the road absorbs doesn’t effect surrounding landscape. Costs loads. Altered hydrology of the system. Destroyed research sites. Road is a barrier

In long run cumulative effect of such activities will cause biodiversity losses and reduce arctic wilderness heritage considerably. eg road block the movement of small animals, expose large animals to heavy hunting pressure, and poaching and cause sedimentation in ricers from erosion.

Cumulative impacts more serious in the arctic too bc the permafrost magnifies disturbances and makes restoration efforts difficult or impossible

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5
Q

Wilderness areas in Norway

A

Wilderness: areas lying 5km or more from roads, railways, and regulated water courses. During the last century undisturbed or pristine wilderness areas have reduced from 48% of countryside in 1900 to 11.8% in 1998. Trend largely because of agriculture, forestry, and hydro electric development

Huge fragmentation of landscape. oil funds everything in Norway.

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6
Q

Urban ecology

A

Integrates natural and social sciences to study these radically altered local environments and their regional and global effects.

Ecologists shunned urban areas for most of the 1900s with the result that the ecological knowledge contributed little to solving urban environmental problems.

Pic of graph of people living in urban env

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7
Q

Global change and urban ecosystems

A

Grimm et al

Focussed on 5 major tees of global environmental change that affect and are affected by urban ecosystem

  • change in land use cover
  • biogeochemical cycles
  • climate
  • hydrosystems
  • and biodiversity

Unprecedented rates of urban population growth over past century ave occurred n <3% on the global terrestrial surface and yt, the impact has been global

78% of C emissions,
60% of residential water use
76% of wood used for industrial purposes
attributed to cities

Land change to build cities and support the demand of urban population that drives other types of environmental change

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8
Q

Issues of habitat fragmentation studies

A
  • difficult to interpret
  • measurement of patch rather than at landscape scale
  • most measure fragmentation in ways that do not distinguish between habitat loss and fragmentation itself

Manipulating a landscape to try and fragment it is difficult. Habitat loss doesn’t necessarily mean fragmentation.

  • since habitat fragmentation is a landscape process, sample size is typically only two (one continuous, one fragmented)- so inferences about the effect of fragmentation are weak
  • characterisation of habitat fragmentation is strongly qualitative - each landscape can only be in 2 state = fragmented or continuous
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9
Q

Four effects of fragmentation

A

(a) Reduction in habitat amount
(b) Increase in number of habitat patches
(c) Decrease in sizes of habitat patches
(d) Increase in isolation of patches

((e) creates edges )

Rarely are all four effects considered together. Does it matter what measure of fragmentation a researcher uses? it depends, cannot talk about fragmentation without all 4. When you do one you often do others.

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10
Q

Define habitat fragmentation

A

When a large expanse of a particular, broadly defined habitat ‘type’ is reduced to smaller patches that are isolated by surround, but different, habitats

Surrounding habitat is typically defined at matrix, and in the case of forest fragmentation typically means ‘degraded’ habitat

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11
Q

Implications of the effects of fragmentation

A
  1. Smaller an area often fewer spp it contained
  2. The more isolated a population, less chance immigrants will rescue it from catastrophes etc
  3. Edges allow the invasion of alien spp, make the microclimate intolerable, incr access to humans and lead to cascading ecological effects (eg fire penetration). Can go deep into forests about 100m
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12
Q

Destruction and degradation

A

The primary cause of declines in global biodiversity

Destruction typically leads to fragmentation. Long term changes in structure and function of the remaining habitats.

Biogeography of oceanic islands provided early theoretical framework to understand effect of fragmentation. ‘islands and sea’

Central to controversy has been the lingering uncertainty about the role of decr fragment size and incr isolation relative to the widespread and pervasive effects of habitat loss in explaining declines of biodiversity and degradation of ecosystem.

fragmentation has multiple, simultaneous, interwoven effects that can operate over potentially longterm scales. Rigorous designs and long term implementation of studies can overcome limitations of observational studies. One spans 35 years on 5 continents

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13
Q

The worlds Forests and fragmentation

A

Satellite data can reveal info about human activity and ho it is affecting he landscape. Lost >1/3rd of forest cover worldwide –> likely to suffer from fragmentation

Analysis revealed nearly 20% of the worlds remaining forest is within 100m of an edge

More than 70% are within 1km of forest edge. Most forests are well within the range where human activities alter microclimate, and non-forest spp may influence and degrade forest ecosystems.

Largest contiguous expanses of forests are in the humid tropical regions of the amazon and congo river basins. Large areas of more disjunct forest in SE Asia, New Guinea, and the boreal biomes

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14
Q

Brazil amazon vs brazil atlantic rainforests

A

Brazil amazon

  • rapidly changing frontier, yet most forests remain contiguous and far from edge despite recent increases in fragmentation
  • forest proportion further than 1km from the forest edge decreased from 95% to 75%

brazil atlantic

  • largely deforested landscape, cleared for agriculture and logged for timber over the past 3 centuries. Remaining forest dominated by small fragments, most small than 100ha and within 1000m of forest edge
  • within 1km from edge forest decr from 90% (historically) to <9% today

Ha = 100x100m

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15
Q

Why are long term experiments better

A

dont have issues that come with observational eg

  • lack of rigorous controls
  • replication
  • randomisation
  • or baseline data

Observational have limited ability to isolate the effect of fragmentation from concomitant habitat loss and degradation

Remnant fragments are embedded in different types and quality of surrounding habitats also influences biodiversity and ecosystem production

eg time dynamics- slash and burn agriculture- how long they are there will impact how degraded the habitat is, eg if ALL nutrients removed= worse

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16
Q

Long term fragmentation experiments

A

Image on essay cues

They manipulate species components and control for confounding effects

Long term experiments can detect lagged and chronic impacts

Summary of their findings:

  • reduced area, increased isolation and increased proportion of edge habitat reduced seed predation and herbivory
  • incr proportion of edge increased fledging predation that had the effect of reducing bird fecundity
  • reduced fragment area and increased isolation reduced abundance of birds, mammals, insects, and plants. perhaps bc of reduced movement and abundance, and ability of spp to persist lower. Often entire communities changes

Tropical forests
- reduced fragment size and increased proportion of edge habitat caused shifts in the physical environment that led to the loss of large, old trees in favour of pioneer trees with subsequent impact on community composition and insects

Grasslands
- fragment size also affected succession rate, such that increase light penetration altered seed pools in smaller fragments and impeded the rate of ecological succession relative to larger fragments

All aspects of fragmentation degraded function including reduced C and N retention, productivity, and pollination

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17
Q

Delayed effects of fragmentation on ecosystem degradation

A

(A) The extinction debt represents a delayed loss of species due to fragmentation.

(B) The immigration lag represents differences in species richness caused by smaller fragment area or increased isolation during fragment succession.

(C) The ecosystem function debt represents delayed changes in ecosystem function due to reduced fragment size or increased isolation.

As predicted by theory (36), the extinction debt appears to
take longer to pay in larger fragments.

After more than a decade, immigration lags resulted in 5% fewer species after 1 year, and 15% fewer species after 10 years in small or isolated fragments compared to large or connected fragments (Fig. 4B).

An ecosystem function debt is manifest both as delayed changes in nutrient cycling and as changes to plant and consumer biomass. Loss of function amounted to 30% after 1 year, rising to 80% after a decade in small and isolated fragments when compared to larger and more connected fragments (Fig. 4C). Functional debts can result from biodiversity loss, as when loss of nutrients and reduction in decomposition are caused by simplification of food webs. Alternatively, the impact is exhibited through pathways whereby fragmentation changes biotic (for example, tree density in successional
systems) or abiotic conditions (for example, light regimes or humidity) in ways that alter and potentially impair ecosystem function eg carbon soil dynamics

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18
Q

How much does fragmentation reduce biodiversity by

A

An experiment spanning multiple biomes, scales, 35 years, and 5 continents demonstrates that fragmentation reduces biodiversity by 13-75% and impairs key ecosystem functions by decr biomass and altering nutrient cycles

Effects greatest in smallest and most isolated habitats, and they magnify over time

Need to improve landscape connectivity! bc reduce extinction rates and help maintain ecosystem services

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19
Q

New foci are emerging for studying ecosystem fragmentation including

A
  1. synergies between fragmentation and global changes
  2. eco-evolutionary response of spp to fragmentation
  3. ecological responses to fragmentation in production landscapes - ecosystems who’s services are under extreme appropriation by humans

Conclusions from experiments thus far prolly conservative bc impacts from other environmental changes have mostly been excluded. Most forms of global changes known to reduce pop size and biodiversity will be exacerbated by fragmentation, including CC, invasive spp, hunting, pollution (including light and noise and chemicals ) and altered disturbance regimes

20
Q

What are edge effects

A

Changes in population or community structures that occur at the boundary of 2 habitats.

Areas with small habitat fragments exhibit especially pronounced edge effects that may extend throughout the range. Edge effects vary per habitat, often diminishing the further away from the edge you get

21
Q

What might promote edge effect variability

A
  • age of habitat edges
  • combined effects of multiple nearby edges
  • structure of adjoining matrix veg
  • seasonality
  • influx of animals/propagules from surrounding degraded lands,
  • extreme weather events
  • fires
22
Q

Initial impacts of edge creation

A

Strong micro-climate changes near newly formed edges which are highly permeable to the penetration of heat, light, and wind from outside degraded lands

Most trees at newly formed edges are not physiologically acclimated to the sudden heat and desiccation stress and many drop their leaves and die standing. Overtime the edge is partially sealed by proliferating vine and second growth and microclimate gradients lessen in intensity

Elevated tres mortality drives changes in other phenomena , especially those related to intensity and pace of floristic change in fragments

Abrupt artificial boundaries are especially vulnerable to windstorms that can exert strong lateral shear forces on exposed trees and create downwind turbulence.

Periodic droughts can also contribute to vulnerability and temporal variability. Structure and composition of adjoining matrix veg can have strong influence on EE.

Striking variability suggests short term experience may fail to detect important phenomena or may characterise them inadequately

Has been suggested known penetration distance of EE should be x2ed for management purposes such as when designing buffer zones for nature reserves

23
Q

Plots with 2 or more edges

A

Such as those in small (1ha) fragments and on the corner of larger fragments have significantly greater tress mortality and biomass loss, and fewer old-growth tree seedling. Higher abundance of pioneer and invasive tree spp, and lianas too. Than those with just one edge

24
Q

how much forest globally is degraded, secondarily or heavily logged

A

> 60%

Lots of potential to allow these forest to grow back, regenerate to become sinks again

Conical tress indicate heavily logged area- haven’t had chance to grow to fill canopy

25
Q

The case for afforestation and reforestation

A

Afforestation is the establishment of a forest or stand of trees (forestation) in an area where there was no previous tree cover

A more converted land becomes degraded and abandoned, opportunities exist to reforest or newly create forests. Marginal agricultural land may not longer be profitable to farm. Could connect back. Shift back to c sinks

26
Q

Difference between primary and secondary forests

A

Primary

  • more epiphyte-richness (plants that grow on other plants) and species abundance
  • more carbon stored. Older, bigger trees, denser wood
  • more structurally complex, more species packed in per unit volume of forest. More photosynthesis

Secondary - what we get when we restore deforested areas

  • less c stored (trees smaller and younger). Get a lot of fast growing spp who’s wood tends to be less dense.
  • lower primary productivity
  • can regain ecosystem functions and elements of biodiversity- better than not having any forest at all
27
Q

Forest regeneration pic

A

Can be natural (successional) or via restoration (tree planting). But which one depends on cost, state of area left etc

POP

If it had been agriculture it could be nutrient deprived, far from other forests to immigrate into so would have to manually intervene in restoration.

Less degraded areas (partially filled) may have natural dispersal opportunities, could use fragments to grow up native trees and fill gaps

28
Q

How can you quickly establish a canopy

A

Fast growing native and alien spp

eg costa rica

29
Q

How can alien pioneers help forest regeneration

A

can act as nurse tree for native hardwoods.

Amani nature reserve in tanzania example of this

Maesopsis eminii has now become widespread throughout East Usambara Mountains

A bird has also invaded because it likes the fruit.

The spp is invasive but it has been helpful to rehabilitate the forest. It is an early succession species and will end up being succeeded by native spp

Regeneration can be trial and error. Trying to find fast growing pioneer spp can be difficult. This allows other spp of plants to come in via animals. Positive feedback where natural regeneration can occur

30
Q

Locking up carbon and conserving biodiversity

A

Carbon based payments for ecosystem services

Carbon storage enhancement from secondary forests regenerating on abandoned farmland. Selling carbon credits. So allow regeneration then can use the credits to pay for things like community projects.

Need to meet certain standards to be able to sell your carbon. Can sign up to verified programme. As part o the projects have to benefit local communities as well as serving biodiversity. Regenerate land that isnt that productive for farming.

More than 200 million tonnes of GG emissions have been removed by this scheme.

31
Q

Can secondary forests match primary carbon stocks ?

A

With time, C stocks can approach the level of primary. After about 30 years in one experiment. POP

Still much lower soil carbon stocks than natural forests (even after 56 years). Difference less pronounced for above ground biomass. Takes more time for below ground carbon stores to build up

32
Q

Can secondary forests have similar diversity to primary

A

Similarity of bird spp low in young 2 forest. Advanced 2 better

Insects show similar trend

read Gilroy et al. (2014) Nature Climate Change 4: 503-507

Overtime as 2 incr in age we have more vulnerable spp approaching the levels we see in primary forests. However, still likely to miss a lot of unique species

In primary more than half spp unique to the habitat

33
Q

What are the forests limits to regaining diversity and function in secondary forests? What cant we get back

A

Cant get back peat stores that were slowly accumulated. Then lost through burning

Spp unique to a location might go extinct. May go extinct with initial deforestation, or may be ongoing extinction that occurs from fragmentation. Or if species can expand beyond fragmented range even reforestation attempts won’t help. –> particularly if they are specialists

Loss of endemic spp. May end up with predominantly exotic, invasive (better dispersing) spp. More abundant generalist spp compared to primary forests.

Structurally very different to primary. Absense of emergent trees, deadwood, structural complexity.

34
Q

Pre-agricultural use of fire

A

Mesolithic people in eu may have used fire to clear forests and remote growth of browse attractive to herbivores

No direct evidence- principally coincident between occurrences of charcoal in sediments and archaeological evidence of people plus modern ethnographic parallels (where these things still occur)

Stronger evidence for deliberate use of fire to manage landscape by prehistoric aboriginal people of australia. Long history oral and written using fire to manage the landscapes. In Aus natural vegetation is fire resistant bc of prevailing regime of natural fires. Some seeds even need smoke to germinate.

35
Q

Agricultural land use

A

As agriculture developed, human societies became more settled with increased persistent impacts on land cover. Most extreme transformations involve clearance of the forest and replacement by crops or pastures

  • forest clearance began in sw asia in early holocene
  • spread across eu to nemoral zone by mid holocene (5-6000ya)
  • since mid-holocene an incr proportion of eu forest has been cleared and replaced by crop grass and heathland
  • similar elsewhere in world where agriculture developed
  • still have big impacts

SE asia rice cultivation developed by pre-histoic people

N, central and S america where pre-columbian people cultivated a range of crops incl. maize, squash, and various solanacaea

Historically widespread eu settlement has resulted in european style agriculture being practised on almost every continent, with resulting rapid and extensive land surface transformation. We have been moving stuff for a while but at a much slower pace

36
Q

What is albedo

A

“whiteness” the reflectivity of the surface, differs between vegetation types, vegetated and un veg surfaces

Lower albedo= more incoming radiation absorbed. Surface warms more and vice versa. Incr warmth then transferred in part to the atmosphere

  • as sensible heat- by conduction, convection and radiation
  • as latent heat- h20 is evaporated rom the surface and transpired by the veg

Grassland has higher albedo than the forest generally so the forest heats the overlying atmosphere more than grassland. Cropland has similar albedo to grassland when crop mature, however when cut albedo drecreases as soil surface is exposed. Depending on soil type depends on strength of albedo.

Those rich is hummus have low albedo.
Others higher in semi arid areas and when dry

Snow has very high albedo, in forests snow falls through the canopy and therefore albedo still low (apart from when wet and snow sticks to branches and freezes in place)
Contrast in important in spring when insolation (total amount of solar radiation) is high but snow cover persists.

37
Q

What is surface roughness length

A

Relates approximately to height of veg and determines the height above the ground at which windspeed is theoretically 0.

Roughness of earths surface causes drag. If you have a forest you get lots of turbulence and it propagates up.

Turbulent flow -eddies- have a major role in transporting energy and water vapour from the atmosphere just above the ground to higher levels.

Energy transfer to atmosphere is thus less effective in forested areas than grassland, and less effective in grassland than bare soil/snow. People are planted trees back bc less erosion from wind.

38
Q

Interception

A

Water falling as ppt is slowed or preventing from reaching the ground by vegetation, such as when snow accumulates on the forest canopy

Interception higher in veg with higher leaf area index. Re-evaporation of intercepted rainfall returns water vapour to the atmosphere directly. With forests much greater proportion of rain goes into soil

39
Q

What does forest clearance do

A

Reduces transpiration and interception. The downwind atmosphere is drier, generating reduced rainfall. Runn off to streams also increases

  • incr rates of erosion, incl soil erosion
  • peak discharge rates incr
  • a smaller proportion of rain enters soil reservoir
  • an area moist enough naturally to support forest may become moisture deficient following clearance
40
Q

Carbon cycle

A

Forest clearance and burning, or burning of cleared material immediately transfers C sequestered in the biomass to the atmosphere.

Forest clearance accounts fo about 10-30% of current anthropogenic additions of CO2 to the atmosphere. 70% is fossil fuels.

Transformation of forests to grassland or cropland results in reduced biomass compared to pre-existing forest, or forest regenerated after natural fires.

In addition, photosynthetically fixed carbon is cycled more quickly back to the atmosphere with less accumulating as soil c. Soil c, abundant in forests is progressively depleted, increase the overall transfer of carbon to the atmosphere resulting from forest clearance

41
Q

Manipulation of forest fire frequencies

A

Scale of manupulation of fire frequencies today is unprecedented. Fire is used to manage large areas used for livestock grazing. Usually to prevent encroachment of woody vegetation.

Many areas burned as much as x10 more often than natural fire regime- some grazing land is being burned annually. Carbon back to the atmosphere to affect global climate - black carbon deposition on snow and ice lowers albedo and accelerates melting.

Fire prevention is practised too in areas where natural fire freqs higher than ideal. eg decades. Often where human settlements are eg mediterranean, aus, calofironia. Also some part of the management plan for PA in yellowstone, mankwe

Leads to accumulation of fuel such that when a fire eventually does occur it is intense and more likely to prove uncontrollable and destructive. Transforming the landscape over a large area and in some cases burning soil c as well as above ground biomass. Potentially sufficiently intense to inject smoke into the upper atmosphere and thus affect climate.

42
Q

Burning the moors

A

At the moment burn them for grouse to bring about new saplings for grouse.

But burning reduces productivity and regeneration capacity.

43
Q

Carbon on snow experiment

A

Got 1 g of black carbon

Spread it out

Snow melted down by 15cm bc albedo. We are contaminating surface of snow dramatically from what goes on in Eu. Melting pressure big- not cc but anthropogenic products.

IPCC have said soot affect on snow albedo may be responsible for a quarter of observed global warming

44
Q

yellowstone fire

A

eg fire in yellowstone 1998 clover mist fire burned from july 9th to september. Consuming for than 570km2

45
Q

Why would fresh water be impounded

A

power generation, reservoirs, water supply, irrigation for agriculture

46
Q

What does impoundment do

A

buffers peak flows and reduces water flow generally

  • causes deposition of suspended material eroded further upstream

incr downstream erosion rates

  • prevents movement of migratory fish eg yangtze paddlefish - unless appropriate measures taken

Generates large water bodies that modify local climates

  • in higher latitude areas act as seasonal store of thermal energy, reducing frost incidence and incr minimum temp in the surrounding landscape
  • lower latitude areas reduce summer temp mama and incr humidity in the surrounding landscape
  • larger the reservoir the greater the magnitude and extent of these effects eg lake Volta, ghana. At 8482km2 it is the world largest water storage reservoir

What rights to countries have to dam rivers that reduce water flow further down

47
Q

What is the early anthropogenic hypothesis

A

The centrepiece of the early anthropogenic (Anthropocene) hypothesis is the claim that humans took control of greenhouse- gas trends thousands of years ago because of emissions from early agriculture.

A common reaction to this claim is that too few people lived thousands of years ago to have had a major effect on either land use or greenhouse-gas concentrations.

Implicit in this view is the notion that per-capita land clearance has changed little for millennia, but numerous field studies have shown that early per-capita land use was large and then declined as increasing population density led to more intensive farming.

Ruddiman et al
Despite four decades of debate over the long term cause-and effect relationship between population increases and agricultural innovations, Boserup’s observation that land use per capita decreases as populations increase has found enduring support.